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<article language="en">
	<journal>
		<journal_title>Climate of the Past Discussions</journal_title>
		<journal_url>www.clim-past-discuss.net</journal_url>
		<issn>1814-9340</issn>
		<eissn>1814-9359</eissn>
		<volume_number>6</volume_number>
		<issue_number>1</issue_number>
		<publication_year>2010</publication_year>
	</journal>
	<doi>10.5194/cpd-6-1-2010</doi>
	<article_url>http://www.clim-past-discuss.net/6/1/2010/</article_url>
	<abstract_html>http://www.clim-past-discuss.net/6/1/2010/cpd-6-1-2010.html</abstract_html>
	<fulltext_pdf>http://www.clim-past-discuss.net/6/1/2010/cpd-6-1-2010.pdf</fulltext_pdf>
	<start_page>1</start_page>
	<end_page>18</end_page>
	<publication_date>2010-01-06</publication_date>
	<article_title content_type="html">Characteristics of cold-warm variation in the Hetao region and its surrounding areas in China during the past 5000 yr</article_title>
	<authors>
		<author numeration="1" affiliations="1,2">
			<name>M. Li</name>
		</author>
		<author numeration="2" affiliations="1">
			<name>Q. Ge</name>
			<email>geqs@igsnrr.ac.cn</email>
		</author>
		<author numeration="3" affiliations="1">
			<name>Z. Hao</name>
		</author>
		<author numeration="4" affiliations="1">
			<name>J. Zheng</name>
		</author>
		<author numeration="5" affiliations="1,2">
			<name>S. He</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Institute of Geographical Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing 100101, China</affiliation>
		<affiliation numeration="2" content_type="html">Graduate School of the Chinese Academy of Sciences, Beijing 100049, China</affiliation>
	</affiliations>
	<abstract content_type="html">Using six long-term temperature proxy data series derived from
      different natural evidences, including pollens and
      lake-sediments, we reconstructed a temperature series with
      a 100-year time resolution for the past 5000 yr in the Hetao
      region and its surrounding areas. The resulting series
      suggests that, on a millennial timescale, temperatures in the
      region were higher than the mean value of the whole series
      during the 5000~2600 yr before present (yr BP) period,
      and became relatively low comparing with the average
      temperature of the whole series after 2600 yr BP. Within
      these two periods, temperature fluctuations comprising
      numerous short, multi-centennial intervals also
      existed. A comparison between our reconstructed series and
      other series in China and across the Northern Hemisphere
      indicate that, on a long-term scale, cold–warm variations had
      been in phase across the whole hemisphere during the past
      5000 yr; on the century to multi-century scale, the beginning
      and the ending times varied from region to region, thus
      implying that climate changes did not occur simultaneously in
      different regions.</abstract>
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